4.7 Article

Sensitivity analysis of the surface ozone and fine particulate matter to meteorological parameters in China

Journal

ATMOSPHERIC CHEMISTRY AND PHYSICS
Volume 20, Issue 21, Pages 13455-13466

Publisher

COPERNICUS GESELLSCHAFT MBH
DOI: 10.5194/acp-20-13455-2020

Keywords

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Funding

  1. National Key R&D Program of China [2016YFC0203500, 2018YFC0213800]
  2. National Natural Science Foundation of China [41975162, 41675125, 41705102]
  3. Jiangsu Environmental Protection Research Project [2016015]

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Meteorological conditions play important roles in the formation of ozone (O-3) and fine particulate matter (PM2.5). China has been suffering from serious regional air pollution problems, characterized by high concentrations of surface O-3 and PM2.5. In this study, the Community Multiscale Air Quality (CMAQ) model was used to quantify the sensitivity of surface O-3 and PM2.5 to key meteorological parameters in different regions of China. Six meteorological parameters were perturbed to create different meteorological conditions, including temperature (T), wind speed (WS), absolute humidity (AH), planetary boundary layer height (PBLH), cloud liquid water content (CLW) and precipitation (PCP). Air quality simulations under the perturbed meteorological conditions were conducted in China in January and July of 2013. The changes in O-3 and PM2.5 concentrations due to individual meteorological parameters were then quantified. T has a great influence on the daily maximum 8 h average O-3 (O-3-8 h) concentrations, which leads to O-3-8 h increases by 1.7 in January in Chongqing and 1.1 ppb K-1 in July in Beijing. WS, AH, and PBLH have a smaller but notable influence on O-3-8 h with maximum change rates of 0.3 ppb %(-1), -0.15 ppb %(-1), and 0.14 ppb %(-1), respectively. T, WS, AH, and PBLH have important effects on PM2.5 formation of both in January and July. In general, PM2.5 sensitivities are negative to T, WS, and PBLH and positive to AH in most regions of China. The sensitivities in January are much larger than in July. PM2.5 sensitivity to T, WS, PBLH, and AH in January can be up to -5 mu gm(-3) K-1, -3 mu gm(-3)%(-1), -1 mu g m(-3) %(-1), and +0.6 mu g m(-3) %(-1), respectively, and in July it can be up to -2 mu g m(-3) K-1, -0.4 mu g m(-3) %(-1), -0.14 mu g m(-3) %(-1), and +0.3 mu g m(-3) %(-1), respectively. Other meteorological factors (CLW and PCP) have negligible effects on O-3-8 h (less than 0.01 ppb %(-1)) and PM2.5 (less than 0.01 mu g m(-3) %(-1)). The results suggest that surface O-3 and PM2.5 concentrations can change significantly due to changes in meteorological parameters, and it is necessary to consider these effects when developing emission control strategies in different regions of China.

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